Rubidium strontium age dating

Episodes of global volcanic activity, rifting of continents, folding, and metamorphism are defined by absolute ages.

The results suggest that the present-day global tectonic scheme was operative in the distant past as well.

The utility of the rubidium–strontium isotope system results from the fact that Sr with a half-life of 49.23 billion years.

To date past events, processes, formations, and fossil organisms, geologists employ a variety of techniques.A coin, vessel, or other common artifact could link two archaeological sites, but the possibility of recycling would have to be considered.It should be emphasized that linking sites together is essential if the nature of an ancient society is to be understood, as the information at a single location may be relatively insignificant by itself.Without absolute ages, investigators could only determine which fossil organisms lived at the same time and the relative order of their appearance in the correlated sedimentary rock record.Unlike ages derived from fossils, which occur only in sedimentary rocks, absolute ages are obtained from minerals that grow as liquid rock bodies cool at or below the surface.

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In the ideal case, the geologist will discover a single rock unit with a unique collection of easily observed attributes called a marker horizon that can be found at widely spaced localities.

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